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William F Cain

Biographic Data

ID5601560
NAMEWilliam F Cain
GIVEN NAMESWilliam F
FAMILY NAMECain
SIGNATURECAIN W F
VERIFIEDNo
TOTAL WORKS1
TOTAL CITATIONS4
AUTHOR COUNT1
EDITOR COUNT0
FIRST PUBLICATION YEAR2018
LATEST PUBLICATION YEAR2018
H-INDEX1
  • Uptake of Carbon for Cellulose Production in a White Oak from Western Oregon, USA

    Open Access•William F Cain, Sheila Griffin et al.•ARTICLE•Radiocarbon•2018•Cited by: 4•References: 13

    We report ∆ 14 C measurements of cellulose extracted from near monthly tree ring growth for the 1960s of a white oak that grew in western Oregon, USA. Comparison with ∆ 14 C measurements of atmospheric CO 2 reveals that the tree ring ∆ 14 C values were equal to or lower than those in atmospheric CO 2 at the time of ring formation. We suggest that the low tree ring ∆ 14 C values during the period 1962–1963 were caused by the presence of an atmosph…

  • Uptake of Carbon for Cellulose Production in a White Oak from Western Oregon, USA

    Open Access•William F Cain, Sheila Griffin et al.•ARTICLE•Radiocarbon•2018•Cited by: 4•References: 13

    We report ∆ 14 C measurements of cellulose extracted from near monthly tree ring growth for the 1960s of a white oak that grew in western Oregon, USA. Comparison with ∆ 14 C measurements of atmospheric CO 2 reveals that the tree ring ∆ 14 C values were equal to or lower than those in atmospheric CO 2 at the time of ring formation. We suggest that the low tree ring ∆ 14 C values during the period 1962–1963 were caused by the presence of an atmosph…

  • Uptake of Carbon for Cellulose Production in a White Oak from Western Oregon, USA

    Open Access•William F Cain, Sheila Griffin et al.•ARTICLE•Radiocarbon•2018•Cited by: 4•References: 13

    We report ∆ 14 C measurements of cellulose extracted from near monthly tree ring growth for the 1960s of a white oak that grew in western Oregon, USA. Comparison with ∆ 14 C measurements of atmospheric CO 2 reveals that the tree ring ∆ 14 C values were equal to or lower than those in atmospheric CO 2 at the time of ring formation. We suggest that the low tree ring ∆ 14 C values during the period 1962–1963 were caused by the presence of an atmosph…

Archaeology (1 works) · Atmospheric sciences (1 works) · Biology (1 works) · Botany (1 works) · Cellulose (1 works) · Chemistry (1 works) · Dendrochronology (1 works) · Environmental Science (1 works) · Forestry (1 works) · Geography (1 works)

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